Global finite-frequency S-wave delay-times: how much crust matters
Author:
Affiliation:
1. Institut de Physique du Globe de Strasbourg, UMR 7516, Université de Strasbourg, EOST/CNRS, F-67084 Strasbourg cedex, France
Funder
Incorporated Research Institutions for Seismology
National Science Foundation
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggz222/28655802/ggz222.pdf
Reference36 articles.
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3. A new method for computing synthetic seismograms;Chapman;Geophys. J. R. astr. Soc.,1978
4. Optimal measurement of relative and absolute delay times by simulated annealing;Chevrot;J. geophys. Int.,2002
5. Fréchet kernels for finite-frequency traveltime–I. Theory;Dahlen;J. geophys. Int.,2000
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1. On accounting for the effects of crust and uppermost mantle structure in global scale full-waveform inversion;Geophysical Journal International;2024-08-06
2. Tomographic filtering via the generalized inverse: a way to account for seismic data uncertainty;GEOPHYS J INT;2020
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